Layers of the earth Flashcards

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1
Q

Outermost layer of the earth

A

Crust

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2
Q

Dense, thin, younger tightly packed and found in
water

A

Oceanic Crust

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3
Q

Thicker and found in lava

A

Continental Crust

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4
Q

Holds the continents, the solid and rigid outer
layer
*Composed of the crust and upper asthenosphere

A

Lithosphere

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5
Q

The mostly solid bulk of the earth’s interior

A

Mantle

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6
Q
  • Semi solid and ductile, tectonic
    plates move on top of this layer. Holds convection currents.
A

Upper Mantle / Asthenosphere

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7
Q
  • Pressure is so great that rocks move
    slower.
A

Lower Mantle / Mesosphere

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8
Q
  • Innermost layer of the planet
A

Core

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9
Q

As hot as the sun, is solid due to high pressure.
Contains hardened iron

A

Inner core

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10
Q
  • Less pressure allows it to stay liquid form. Has
    melted iron and nickel and makes up most of the core.
A

Outer core

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11
Q

This theory believes in the fact that all continents were once
part of a bigger continent called Pangea
- This is supported by:
a.Similar landscape across different islands
b.Continents looking like puzzle pieces separated
c. Fossils of terrestrial animals spread across islands
- Discovered by Alfred Wegener
- The proof would come far later in the future through…

A

The Continental Drift Theory / Pangea Theory

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12
Q
  • A theory that dives deeper into the “Why” aspect of the
    pangea theory
  • This theory states that the convection currents are the reason
    for the drifting of the continents
  • Using a seismograph, scientists discovered the plate margins
    that run across the globe, splitting the world into the
    continents.
  • Seismograph measures seismic waves releasing from plate
    margins.
  • It is through these plate margins that the convection currents
    are released, causing the formation of different landscapes
A

The Tectonic Plate Theory

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13
Q

A theory that explains how the tectonic plate theory affects
the landscape.
- When the oceanic and continental crust converge, the oceanic
crust goes underneath the continental crust due to its density.
- That process is called subduction and a subduction zone is the
zone where the oceanic crust sinks due to its density.
- The oceanic crust gets closer to the mantle where it burns
due to the convection currents
- After burning, the lava flows in the mantle until it finds a plate
margin underwater to pour out of
- In the plate margins, lava flows out turning into magma
which pushes the oceanic crust into the continental crust,
thus creating more lava in the process
- Convergent plates of oceanic and continental are what cause
the movement of continents because as the seafloor widens,
so does the gap between plate margins

A

Seafloor Spreading Theory

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14
Q

Results in the oceanic crust sinking and melting before
reemerging in the plate boundaries.
- Responsible for the drifting of continents

A

Convergent Boundaries (Oceanic to Continental)

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15
Q

Are responsible for the formation of mountains
- Also creates a subduction zone

A

Convergent Boundaries (Continental to Continental)

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16
Q

The denser crust sinks and forms another subduction zone
- As the denser crust sinks, some fluids are released and
partially melt the ingenious rock, possibly rising and erupting
as underwater volcanoes

A

Convergent Boundaries (Oceanic to Oceanic)

17
Q

Occurs when two tectonic plates separate and pull away,
forming valleys, mountain wrangler, and rift valleys
- In oceanic crust divergent boundaries, the magma leaks out
of the plate boundary, cooling into magma

A

Divergent Boundaries

18
Q

Happens when the tectonic plates slides in opposite
directions, like a two trains in a subway
- Fault lines and rift valleys are also a result of this

A

Transform Boundaries

19
Q

are caused through convergent boundaries in
subduction zones where the motion of the plates build
pressure
- Overtime, the pressure will be too much for the rocks to
handle and the energy will release at once, causing
earthquakes

A

Earthquakes

20
Q

formed in underwater earthquakes where the
pressure makes a huge wave

A

Tsunamis

21
Q

The cycle of heat found in the asthenosphere

A

Convection Currents

22
Q
  • The tool used to measure seismic waves
A

Seismograph

23
Q

Edge of a tectonic plate, usually where plates drift away or
against each other

A

Plate Margins

24
Q
  • The quantity of vibrations coming from the build up of
    pressure in the mantle
A

Seismic Waves

25
Q

The process in which a tectonic plate sinks beneath another
plate due to a convergent boundary

A

Subduction

26
Q

A word for when plate tectonics collide with each other

A

Converge

27
Q

The area in which a tectonic plate sinks beneath another plate

A

Subduction Zone

28
Q

Usually found in the ocean and is more or less cooled down
lava

A

Igneous Rock

29
Q

Plates that are separated by the plate margins and usually
hold the continents

A

Tectonic Plates